The Hanoverton plate. Relief from Copernicus GLO-30; rivers and lakes from USGS NHD; watersheds from the USGS Watershed Boundary Dataset; roads and city limits from Census TIGER 2024.
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Hanoverton’s center stands about 1,160 ft above sea level. Within three miles the land runs from 1,110 ft to 1,340 ft, a difference of 230 ft: rolling country. The highest named summit within 15 miles is Round Knob, about 1,440 ft, 15 miles east-southeast.
Under the town center the state geologic map shows Allegheny and Pottsville Groups, Undivided (shale, siltstone), from the Carboniferous, 299 to 324 million years old.
The section below crosses 2 rock units mapped at the surface.
Heights every 0.1 mile from the Copernicus GLO-90 surface model; vertical exaggeration about 46×. The colored band under the surface is the rock the state geologic map shows at the surface, not a picture of what lies beneath.
Shale, siltstone, mudstone. Age: Carboniferous, 299 to 324 million years old. About 17 mi of the line.
Shale, siltstone. Age: Carboniferous, 299 to 324 million years old. About 7 mi of the line.
From the USGS State Geologic Map Compilation (Horton and others, 2017), the states’ geologic maps joined at a common scale.
Heights from Copernicus GLO-90 (a surface model: it includes buildings and tree canopy); summits from USGS GNIS; rivers from USGS NHDPlus HR; rock from the USGS State Geologic Map Compilation.
A raindrop that lands in Hanoverton reaches the Gulf of America by way of Sandy Creek, the Tuscarawas, the Muskingum, the Ohio and the Mississippi: about 2,000 river miles.
970 miles of the trip are on the Mississippi.
Traced down the USGS NHDPlus V2.1 river network from the Census center point of Hanoverton; river miles along the main stem, rounded.
